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脉冲光加热热反射法与激光加热金刚石压腔相结合用于原位高压-高温热扩散率测量。

Combination of pulsed light heating thermoreflectance and laser-heated diamond anvil cell for in-situ high pressure-temperature thermal diffusivity measurements.

作者信息

Hasegawa Akira, Yagi Takashi, Ohta Kenji

机构信息

National Metrology Institute of Japan, National Institute of Advanced Industrial Science and Technology, Tsukuba, Ibaraki 305-8563, Japan.

Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, Tokyo 152-8551, Japan.

出版信息

Rev Sci Instrum. 2019 Jul;90(7):074901. doi: 10.1063/1.5093343.

Abstract

By combining thermoreflectance measurements and laser heated diamond anvil cell (LHDAC) techniques, an instrument for the measurement of in situ high pressure-temperature thermal diffusivity of materials was developed. In an LHDAC system, high-power continuous-wave laser beams irradiate both faces of a disk-shaped metal sample loaded into diamond anvil cells (DACs), to maintain a stable high-temperature condition. During the operation of the LHDAC system, temperature of the sample is determined from the thermal radiation spectrum between 640 and 740 nm to fit Planck's law. Subsequently, a pulsed laser beam irradiates the metal disk to induce a temperature gradient inside the sample, and the transient temperature, caused by heat diffusion, is measured by a continuous wave probe laser based on the thermoreflectance phenomenon. We determined the thermal conductivities of Pt and Fe up to approximately 60 GPa and 2000 K using the measured thermal diffusivities and obtained values consistent with previous works. The uncertainties in the pressure and the temperature are estimated to be approximately 10%, and that in the thermal conductivity is estimated to approximately 15%. The system developed in this study enables us to determine thermal transport properties of materials under pressure-temperature conditions of the deep Earth.

摘要

通过结合热反射测量和激光加热金刚石对顶砧(LHDAC)技术,开发了一种用于测量材料原位高压 - 温度热扩散率的仪器。在LHDAC系统中,高功率连续波激光束照射加载到金刚石对顶砧(DAC)中的盘形金属样品的两面,以维持稳定的高温条件。在LHDAC系统运行期间,根据640至740nm之间的热辐射光谱确定样品温度以符合普朗克定律。随后,脉冲激光束照射金属盘以在样品内部诱导温度梯度,并且基于热反射现象通过连续波探测激光测量由热扩散引起的瞬态温度。我们使用测量的热扩散率确定了高达约60GPa和2000K的Pt和Fe的热导率,并获得了与先前工作一致的值。压力和温度的不确定度估计约为10%,热导率的不确定度估计约为15%。本研究中开发的系统使我们能够确定在地球深部压力 - 温度条件下材料的热传输特性。

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